FEN BİLİMLERİ ENSTİTÜSÜ/LİSANSÜSTÜ TEZ PROJESİ

FEN BİLİMLERİ ENSTİTÜSÜ/LİSANSÜSTÜ TEZ PROJESİ Doğan, Musa(2015-12-31) A NUMERİCAL TAXONOMİC STUDY ON THE GENUS SALVİA L. ( LAMİACEAE) IN TURKEY
FEN BİLİMLERİ ENSTİTÜSÜ/LİSANSÜSTÜ TEZ PROJESİ Akkaya, Mahinur; Dagvadorj, Bayantes(2014-12-31) GENE-FUNCTION ANALYSIS OF CANDIDATE EFFECTOR PROTEINS OF WHEAT STRIPE RUST PATHOGEN
Orta Anadolu Geç Pliyosen İklimi: Pınarbaşı Tufalarından (D Kayseri) Sedimantolojik, Mikroskopik ve İzotopik Bulgular Ocakoğlu, Faruk; Yılmaz, İsmail Ömer (2015-11-08) 100 km-long, NE-running Pınarbaşı basin (Central Anatolia, E Kayseri) comprises sporadic, km-scale tufa deposits at its uppermost stratigraphic levels in vicinity of basin margin. Tufa deposits are covered by well-dated, extensive Valibaba tepe ignimbrite (2.52 Ma) following several metres thick fluvial sediments. Sedimentological, stable isotopic, microscopic and magnetic susceptibility (MS) data from tufa outcrops in vicinity of Samağır village at the north of basin provide important con...
MICROFACIES ANALYSIS OF THE EOCENE ÇAYRAZ FORMATION (HAYMANA BASIN, TURKEY): RESPONSE OF BENTHIC FORAMINIFERAL COMMUNITIES TO SEDIMENTARY CYCLICITY Bengül, Nilya; Altıner, Sevinç; Department of Geological Engineering (2022-8-31) The Haymana Basin in central Anatolia (Turkey) formed during the closure of the Neo-Tethys in the Late Cretaceous to Middle Eocene as a forearc accretionary wedge. Middle Eocene aged units in this basin are exposed near Çayraz Village, Haymana. The Çayraz Formation is represented by the package of nummulitic banks and intercalation of calcareous mudstones. The aim of this study to investigate the sedimentary cyclicity and depositional sequences in the Eocene successions of the Haymana Basin. To be able to a...
GEOCHEMISTRY AND PETROGENESIS OF THE ARC-RELATED KÖSDAĞ METAVOLCANICS, SOUTHERN CENTRAL PONTIDES, NORTHERN TURKEY Berber, Faruk; Sayıt, Kaan; Department of Geological Engineering (2021-12-27) The Kösdağ Metavolcanics (KM) in the southern Central Pontides crops out between the Izmir-Ankara-Erzincan Suture Zone (IAESZ) in the south and the Sakarya Composite Terrane in the north. The unit is represented by a low-grade metamorphic assemblage including meta-basics, meta-intermediates, and meta-felsics, interlayered with recrystallized limestone, mudstone, and chert. While the unit is bounded to the north by the North Anatolian Fault Zone (NAFZ), the Dikmen Formation stratigraphically overlie the unit...

Citation Formats

İ. Ö. Yılmaz, “FEN BİLİMLERİ ENSTİTÜSÜ/LİSANSÜSTÜ TEZ PROJESİ,” 2014. Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/60456.